Hi All

There is more on February 09 ice at

http://nsidc.org/arcticseaicenews/

Stephen

Emeritus Professor of Engineering Design
School of Engineering and Electronics
University of Edinburgh
Mayfield Road
Edinburgh EH9 3JL
Scotland
tel +44 131 650 5704
fax +44 131 650 5702
Mobile  07795 203 195
[email protected]
http://www.see.ed.ac.uk/~shs 



John Nissen wrote:
> Talk about unpleasant surprises (see my previous posting below), look at 
> this:
>
> 'Warm everywhere' in Arctic this winter
>
> While parts of North America have been in the icy grips of an unusually cold 
> and snowy winter recently, the Arctic has been downright balmy compared to 
> past winters.
>
> http://www.msnbc.msn.com/id/29038734/from/ET/
>
> (with thanks to Albert Kallio for finding this)
> ----
>
> 'Warm everywhere' in Arctic this winter
> Expert: Dec.-Jan. temps drop, both are 'crucial ice-growing months'
>
> By Andrea Thompson
> updated 5:13 p.m. ET Feb. 5, 2009
> While parts of North America have been in the icy grips of an unusually cold 
> and snowy winter recently, the Arctic has been downright balmy compared to 
> past winters.
>
> These warmer-than-normal temperatures mean that the sea ice in the Arctic is 
> looking pretty anemic, despite the winter season.
>
> Arctic ice goes through a normal cycle of summer thaw and winter re-freeze. 
> In recent decades, however, sea ice has become overall less extensive and 
> thinner, leading to forecasts that in future decades the polar region will 
> be ice-free during summer. The trend looks to be continuing this winter, 
> scientists now say.
>
> Climate swings in any single season are part of Nature, of course. That's 
> why records - warm or cold, wet or dry - get broken. For much of the United 
> States, this winter has been an exceptionally chilly one.
>
> The average temperature for the United States in December, 32.5 F, was 
> almost 1 degree Fahrenheit below the average for the 20th century, according 
> to the National Oceanic and Atmospheric Administration. Much of the West and 
> Midwest had a particularly frigid month, with temperatures plunging several 
> degrees below average.
>
> This winter in the Arctic has been a completely different story.
>
> "It's warm everywhere in the Arctic. It's anomalously warm," said Julienne 
> Stroeve, of the National Snow & Ice Data Center (NSIDC) in Boulder, Colo.
>
> Both December and January have been abnormally warm months, which impacts 
> the cyclical re-freezing of sea ice over the years, because these are "two 
> crucial ice-growing months," Stroeve told LiveScience.
>
> Thinner ice, more melt
> Arctic sea ice hasn't been reaching its former thicknesses and extents in 
> recent years, especially after the dramatic meltdown observed in the summer 
> of 2007, which opened up the fabled Northwest Passage. (This past summer saw 
> the second lowest summer ice area on record.)
>
> That record melting - which left 30 percent less ice in the Arctic than 
> there was at the previous record low - caused the loss of substantial 
> amounts of older ice, which is thicker and generally survives the summer. 
> Older, thicker ice is typically 6.5 to 10 feet (2 to 3 meters) thick, while 
> younger ice is closer to 3 feet (1 meter) in thickness.
>
> Melting exposes more areas of open ocean, which absorbs incoming sunlight 
> that the ice would normally reflect, so there is the potential for a 
> snowball effect, or what scientists call self-reinforcing or feedback. Come 
> winter, the ice that refreezes is thinner, first-year ice, which is more 
> susceptible to melt in the summer, potentially exposing even more open 
> ocean.
>
> "That [thinner ice] typically can all melt out in the summer," Stroeve said.
>
> This year, the future
> That feedback seems to be kicking in, as now "the Arctic is just more 
> dominated by that thinner ice," Stroeve said, adding that unless February 
> and March are much colder than normal, this winter's ice could end up 
> covering less area than normal and be thinner than even in recent years.
>
> So far, this winter has been warmer than last, Stroeve said, and some odd 
> weather patterns cropped up in both December and January that brought ice 
> growth to a standstill. Pauses in the regrowth of ice aren't a new 
> phenomenon - they have happened before, even in much colder winters - but 
> they only exacerbate the current situation in the Arctic by adding yet 
> another mechanism that stagnates ice growth.
>
> In January, these weather patterns created different conditions in different 
> parts of the Arctic. While ice grew southwest of Greenland, it retreated in 
> areas east of Greenland and in parts of the Barents Sea, the NSIDC reported.
>
> While ice is still re-freezing, ice coverage area at the end of January was 
> still 293,000 square miles (760,000 square kilometers) less than the 
> 1979-2000 average, according to the NSIDC. This didn't break the record low 
> for January ice area (set in 2006), but it put January 2009 in the top six. 
> Including this year, January ice area is declining by about 3 percent per 
> decade, the NSIDC reported.
>
> Looking further into the future, unless there are several very cold winters 
> and mild summers, Arctic sea ice is unlikely to bounce back in the coming 
> decades.
>
> "The idea of recovery right now seems pretty slim," Stroeve said. "You just 
> don't get very cold temperatures like you used to."
>
> Eventually, the sea ice is expected to melt out entirely in the summer, 
> leaving only a cover of winter seasonal ice. The NSIDC predicts that this 
> will happen around 2030, though Stroeve says it could happen earlier, as 
> indeed some other scientists predict. That it will happen seems fairly 
> certain: "There's no doubt in my mind about that," Stroeve said.
>
>
> ----
>
> Cheers from Chiswick, where it has been unusually cold and snowy, as in 
> parts of N America,
>
> John
>
>
>
> ----- Original Message ----- 
> From: "John Nissen" <[email protected]>
> To: <[email protected]>
> Cc: "geoengineering" <[email protected]>
> Sent: Friday, February 06, 2009 6:43 PM
> Subject: Re: [geo] Re: runaway arguments ripped to bits
>
>
>   
>> Hi dsw_s,
>>
>> You are right about the relative size of heat flux compared to albedo 
>> effect, but it is the _change_ in heat flux which is important to compare, 
>> e.g. any increased heat flux from the Gulf Stream entering the Arctic 
>> Ocean.
>>
>> Anyway, whatever is the root cause of Arctic shrinkage, it is happening a 
>> lot fast than IPCC predicted only a couple of years ago, and the trend 
>> shows no signs of reversing.  Exactly the opposite - it has shown signs of 
>> accelerating this decade.  There are recognised to be various cycles of 
>> the northern hemisphere ocean-atmosphere system, but we certainly cannot 
>> rely on such a cycle to rescue us by reducing heat flux into the Arctic 
>> and switching off the sea ice retreat.
>>
>> We can indeed expect surprises, but we cannot rely on them being pleasant 
>> ones!  Indeed, most have been extremely unpleasant, of late.  Thus the 
>> urgency for geoengineering is, if anything, increased, taking into account 
>> the precautionary principle.
>>
>> Cheers,
>>
>> John
>>
>>
>> ----- Original Message ----- 
>> From: "dsw_s" <[email protected]>
>> To: "geoengineering" <[email protected]>
>> Sent: Friday, February 06, 2009 1:04 PM
>> Subject: [geo] Re: runaway arguments ripped to bits
>>
>>
>>
>>     
>>> The "forcing" from the sea ice albedo effect is of the order of 30 Watts 
>>> per square metre, so you expect this to drive regional warming.<
>>>       
>> I expect surprises.  How does the total number of watts of forcing
>> compare with variability in heat fluxes into and out of the region?
>> What other feedbacks are there that we haven't thought about?  The
>> vapor pressure over ice is less than over water at the same
>> temperature, and the surface of ice can be cooler than the water
>> below.  So evaporation will presumably be greater over open water than
>> it has been historically over the sea ice.  If that water condenses
>> elsewhere, that's a heat flux out of the region.
>>
>> Let's say we lose ten million square km of sea ice: that's 30
>> terawatts of forcing.  But it looks as though there's over a petawatt
>> of annually-averaged heat flux into the region, just by eyeballing a
>> figure in a badly-out-of-date textbook.  So with even a modest
>> relative change in heat fluxes, the effects of the forcing could show
>> up somewhere else rather than regionally.  Or the regional effects
>> could be an order of magnitude greater than the forcing would produce
>> directly.  For a conclusion about that, I would be more convinced by a
>> peer-reviewed analysis of a detailed model than by the simple-and-
>> obvious argument.
>>
>>
>> On Feb 6, 6:49 am, "John Nissen" <[email protected]> wrote:
>>     
>>> Hi Andrew,
>>>
>>> It depends what kind of proof you want. I myself am convinced of things 
>>> if there is a logical argument based on established facts.
>>>
>>> I am convinced by anthropogenic global warming because if you put an 
>>> extra 100 ppm CO2 in the atmosphere, you EXPECT to have greenhouse 
>>> warming. I don't need "proof" to be convinced. To be persuaded otherwise, 
>>> I would need a convincing explanation of why the CO2 wasn't causing 
>>> global warming, or how this was somehow neutralised. I would need to be 
>>> PROVED WRONG.
>>>
>>> Similarly with methane runaway feedback. There's a vast amount of methane 
>>> trapped in frozen structures. Nobody disputes this fact. If you put 
>>> enough of this methane in the atmosphere, you expect global warming. You 
>>> then expect positive feedback as a result of this, as the frozen 
>>> structures unfreeze to release more methane until it's all gone. Unless 
>>> there is an argument against this logic, I will remain convinced by it.
>>>
>>> Similarly with the Arctic sea ice and domino effects. The "forcing" from 
>>> the sea ice albedo effect is of the order of 30 Watts per square metre, 
>>> so you expect this to drive regional warming. Nobody is suggesting how 
>>> this warming would reverse naturally. So, as the region continues to 
>>> warm, you expect the domino effects of methane release and Greenland ice 
>>> sheet accelerated discharge.
>>>
>>> This is all highly uncomfortable to contemplate, and I'd like to be 
>>> proved wrong. However we do have a possible way out of this situation 
>>> with geoengineering. So all is not lost.
>>>
>>> Please can we now persuade politicians and potential funding bodies of 
>>> the inescapable logic of this situation, so that they fund the necessary 
>>> geoengineering developments? Or prove me wrong.
>>>
>>> Cheers,
>>>
>>> John
>>>       
>
> [snip] 
>
>
> >
>
>   


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